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Ca-rich majorite derived from high-temperature melt and thermally stressed hornblende in shock veins of crustal rocks from the Ries impact crater (Germany)

✍ Scribed by Volker Stähle; Rainer Altherr; Lutz Nasdala; Thomas Ludwig


Publisher
Springer
Year
2010
Tongue
English
Weight
953 KB
Volume
161
Category
Article
ISSN
0010-7999

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